4.7 Article

Small-scale variability patterns of DMS and phytoplankton in surface waters of the tropical and subtropical Atlantic, Indian, and Pacific Oceans

Journal

GEOPHYSICAL RESEARCH LETTERS
Volume 42, Issue 2, Pages 475-483

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1002/2014GL062543

Keywords

dimethylsulfide; phytoplankton; tropical oceans; fluorescence; variability

Funding

  1. Spanish Ministry of Economy and Competitiveness (INGENIO 2010 CONSOLIDER program) [CSD2008-00077]
  2. PEGASO [CTM2012-37615]
  3. U.S. National Science Foundation [0851472, 1143709]
  4. Directorate For Geosciences [1143709, 0851472] Funding Source: National Science Foundation
  5. Div Atmospheric & Geospace Sciences [1143709, 0851472] Funding Source: National Science Foundation

Ask authors/readers for more resources

High-resolution surface measurements of dimethylsulfide (DMS), chlorophyll a fluorescence, and the efficiency of photosystem II were conducted together with temperature and salinity along five eastward sections in the tropical and subtropical Atlantic, Indian, and Pacific Oceans. Analysis of variability length scales revealed that much of the variability in DMS concentrations occurs at scales between 15 and 50 km, that is, at the lower edge of mesoscale dynamics, decreasing with latitude and productivity. DMS variability was found to be more commonly related to that of phytoplankton-related variables than to that of physical variables. Unlike phytoplankton physiological data, DMS did not show any universal diel pattern when using the normalized solar zenith angle as a proxy for solar time across latitudes and seasons. The study should help better design sampling and computing schemes aimed at mapping surface DMS and phytoplankton distributions, taking into account latitude and productivity.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

Article Ecology

Quantifying stratospheric ozone loss over Antarctica in the last two decades using corrected satellite profiles

Shrivardhan Hulswar, Prajakta Mohite, Anoop S. Mahajan

Summary: Loss of stratospheric ozone has occurred due to anthropogenic compounds, and the number of saturated ozone loss events in Antarctica has been studied using satellite observations. The analysis shows a gradual decrease in loss events from 2004 to 2013, followed by no significant trend and strong interannual variation correlated with temperature.

POLAR SCIENCE (2022)

Article Geosciences, Multidisciplinary

The Chemistry of Mercury in the Stratosphere

Alfonso Saiz-Lopez, A. Ulises Acuna, Anoop S. Mahajan, Juan Z. Davalos, Wuhu Feng, Daniel Roca-Sanjuan, Javier Carmona-Garcia, Carlos A. Cuevas, Douglas E. Kinnison, Juan Carlos Gomez Martin, Joseph S. Francisco, John M. C. Plane

Summary: This article presents the first model of stratospheric mercury chemistry and identifies two distinct mercury chemical regimes. The study also reveals that the oxidation of mercury in the stratosphere is faster than previously assumed, but regulated by photo-reduction. The lifetime of mercury in the stratosphere shows a significant variation.

GEOPHYSICAL RESEARCH LETTERS (2022)

Article Geosciences, Multidisciplinary

Substantial contribution of iodine to Arctic ozone destruction

Nuria Benavent, Anoop S. Mahajan, Qinyi Li, Carlos A. Cuevas, Julia Schmale, Helene Angot, Tuija Jokinen, Lauriane L. J. Quelever, Anne-Marlene Blechschmidt, Bianca Zilker, Andreas Richter, Jesus A. Serna, David Garcia-Nieto, Rafael P. Fernandez, Henrik Skov, Adela Dumitrascu, Patric Simoes Pereira, Katarina Abrahamsson, Silvia Bucci, Marina Duetsch, Andreas Stohl, Ivo Beck, Tiia Laurila, Byron Blomquist, Dean Howard, Stephen D. Archer, Ludovic Bariteau, Detlev Helmig, Jacques Hueber, Hans-Werner Jacobi, Kevin Posman, Lubna Dada, Kaspar R. Daellenbach, Alfonso Saiz-Lopez

Summary: The study found that iodine chemistry plays a more important role than bromine chemistry in tropospheric ozone losses in the Arctic. Chemical reactions between iodine and ozone were identified as the second highest contributor to ozone loss over the study period.

NATURE GEOSCIENCE (2022)

Article Multidisciplinary Sciences

Marine biogenic emissions of benzene and toluene and their contribution to secondary organic aerosols over the polar oceans

Charel Wohl, Qinyi Li, Carlos A. Cuevas, Rafael P. Fernandez, Mingxi Yang, Alfonso Saiz-Lopez, Rafel Simo

Summary: Measurements of benzene and toluene in the remote Southern Ocean and the Arctic marginal ice zone suggest a marine biogenic source. Calculated emission fluxes for benzene and toluene in the Southern Ocean were 0.023 +/- 0.030 and 0.039 +/- 0.036 μmol m-2 day-1, while in the Arctic, they were 0.023 +/- 0.028 and 0.034 +/- 0.041 μmol m-2 day-1, respectively. These emissions, previously overlooked, have a significant impact on secondary organic aerosol mass concentrations, particularly over the Southern Ocean.

SCIENCE ADVANCES (2023)

Article Geosciences, Multidisciplinary

Arctic mercury flux increased through the Last Glacial Termination with a warming climate

Delia Segato, Alfonso Saiz-Lopez, Anoop Sharad Mahajan, Feiyue Wang, Juan Pablo Corella, Carlos Alberto Cuevas, Tobias Erhardt, Camilla Marie Jensen, Chantal Zeppenfeld, Helle Astrid Kjaer, Clara Turetta, Warren Raymond Lee Cairns, Carlo Barbante, Andrea Spolaor

Summary: According to ice-core data and atmospheric chemistry modeling, deposition of mercury onto the Greenland Ice Sheet increased during the transition from the Last Glacial Termination to the early Holocene epoch. This increase was associated with regional climate warming and the retreat of sea ice, driven by oceanic mercury evaporation and atmospheric bromine. The findings suggest that climate change may contribute to higher mercury levels in Arctic ecosystems.

NATURE GEOSCIENCE (2023)

Article Multidisciplinary Sciences

Natural short-lived halogens exert an indirect cooling effect on climate

Alfonso Saiz-Lopez, Rafael P. P. Fernandez, Qinyi Li, Carlos A. A. Cuevas, Xiao Fu, Douglas E. E. Kinnison, Simone Tilmes, Anoop S. S. Mahajan, Juan Carlos Gomez Martin, Fernando Iglesias-Suarez, Ryan Hossaini, John M. C. Plane, Gunnar Myhre, Jean-Francois Lamarque

Summary: Observational evidence suggests that ocean-emitted short-lived halogens have a widespread presence in the global atmosphere. These compounds, both naturally emitted and anthropogenically amplified, have a significant cooling effect on Earth's radiative balance. This effect has increased since pre-industrial times and is projected to change further in the future.

NATURE (2023)

Article Limnology

Global Ocean dimethylsulfide photolysis rates quantified with a spectrally and vertically resolved model

Marti Gali, Emmanuel Devred, Gonzalo L. Perez, David J. Kieber, Rafel Simo

Summary: Photochemical reactions initiated by ultraviolet radiation can remove the climate-active gas dimethylsulfide (DMS) from the ocean's surface layer. We quantified DMS photolysis using a satellite-based model that considers spectral irradiance attenuation, absorption by dissolved organic matter, and the apparent quantum yields (AQYs) of DMS degradation. Two alternative parameterizations for AQY estimate global DMS photolysis at 17-20 Tg S yr(-1), of which about 73% occurs in the Southern hemisphere. Simplified schemes used in current biogeochemical models overestimate DMS photolysis by around 150% globally, and we propose relevant corrections and adjustments.

LIMNOLOGY AND OCEANOGRAPHY LETTERS (2023)

Article Ecology

Global analysis of the controls on seawater dimethylsulfide spatial variability

George Manville, Thomas G. Bell, Jane P. Mulcahy, Rafel Simo, Marti Gali, Anoop S. Mahajan, Shrivardhan Hulswar, Paul R. Halloran

Summary: Dimethylsulfide (DMS) emitted from the ocean plays a significant role in our planet's climate. This study investigates the variability of DMS concentrations at local scales and identifies the mechanisms driving this variability. The results show that both physical and biogeochemical processes contribute to DMS variability, with mesoscale eddies playing an important role. The study also highlights the regional differences in DMS variability and suggests that submesoscale features should be considered in DMS models and parameterizations.

BIOGEOSCIENCES (2023)

Article Limnology

Biological sources and sinks of dimethylsulfide disentangled by an induced bloom experiment and a numerical model

Guillaume Le Gland, Marta Masdeu-Navarro, Marti Gali, Sergio M. Vallina, Matti Gralka, Flora Vincent, Otto Cordero, Assaf Vardi, Rafel Simo

Summary: In this study, the dynamics of DMSP and DMS in the ocean and their related biological processes were investigated through experiments and modeling. The results show that phytoplankton blooms can increase DMS emission, but only during a transient regime of a few weeks. Additionally, viral infection has an impact on the production and emission of DMS.

LIMNOLOGY AND OCEANOGRAPHY (2023)

Article Environmental Sciences

Study of atmospheric glyoxal using multiple axis differential optical spectroscopy (MAX-DOAS) in India

Mriganka Sekhar Biswas, Prithviraj Mali, Christophe Lerot, Isabelle De Smedt, Anoop S. Mahajan

Summary: This study investigates the levels of atmospheric glyoxal in three locations in India using Multi-Axis Differential Optical Spectroscopy (MAX-DOAS) observations and compares them to satellite observations. The results show that glyoxal levels are highest in Delhi, lowest in Mahabaleshwar, and similar but slightly lower in Pune compared to Delhi. Pune exhibits significant seasonal variation in glyoxal levels.

ATMOSPHERIC ENVIRONMENT (2023)

Article Geosciences, Multidisciplinary

Third revision of the global surface seawater dimethyl sulfide climatology (DMS-Rev3)

Shrivardhan Hulswar, Rafel Simo, Marti Gali, Thomas G. Bell, Arancha Lana, Swaleha Inamdar, Paul R. Halloran, George Manville, Anoop Sharad Mahajan

Summary: This paper presents an updated estimation of global surface seawater dimethyl sulfide (DMS) climatology with significant improvements in data handling and processing. The results show a decrease in the global annual mean DMS concentration compared to the previous estimation, and large regional differences are observed. The global sea-to-air flux of DMS has also decreased, with the most significant changes occurring in high concentration regions such as the polar oceans.

EARTH SYSTEM SCIENCE DATA (2022)

Review Environmental Sciences

Atmospheric gas-phase composition over the Indian Ocean

Susann Tegtmeier, Christa Marandino, Yue Jia, Birgit Quack, Anoop S. Mahajan

Summary: This article reviews the current progress in detecting and understanding atmospheric gas-phase composition over the Indian Ocean and its impacts on marine ecosystems. The study finds that the changing atmospheric composition over the Indian Ocean can interact with oceanic biogeochemical cycles and impact marine ecosystems, resulting in potential climate feedbacks. However, the impacts of atmospheric pollution on oceanic biogeochemistry and trace gas cycling in the Indian Ocean region are severely understudied.

ATMOSPHERIC CHEMISTRY AND PHYSICS (2022)

Article Environmental Sciences

Substantial loss of isoprene in the surface ocean due to chemical and biological consumption

Rafel Simo, Pau Cortes-Greus, Pablo Rodriguez-Ros, Marta Masdeu-Navarro

Summary: By analyzing ship-based seawater incubation experiments, it was found that the chemical and biological degradation of isoprene in the surface ocean varies with chlorophyll-a concentration. The consumption rates of isoprene in the surface ocean are comparable or greater than ventilation rates to the atmosphere, especially in chlorophyll-a rich waters.

COMMUNICATIONS EARTH & ENVIRONMENT (2022)

No Data Available